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Research advances in the Mesozoic tectonic regimes during the formation of Jiaodong ore cluster area

机译:胶东矿团簇形成过程中的中生代构造体系研究进展

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摘要

Based on research advances of the tectonic regime in Jiaodong ore cluster area and the related tectonic regime transformation in Mesozoic era in the eastern region of North China, in this paper, we first summarize some key problems required to be studied further on. Then we suggest an approach to dealing with these problems. It is known that the gold deposits in Jiaodong ore cluster area, which are of different mineralization styles, spatial distributions and geological settings, might be as a resultfrom one or more geologic events in Mesozoic. Till now, this kind of research on the temporal evolution and spatial migration sequence, especially on the geodynamic mechanism of the above events, is far from sufficient. Moreover, quantitatively describing the action mode and the temporal-spatial framework of tectonic dynamic regimes and formulating the relative contribution of every tectonic dynamic regime for the metallogensis are still challenges to the geologists studying on the formation of Jiaodong ore cluster area. According to the interpretation of the regional tectonic analysis, the structural dynamics, the observation and the exploration of the mineralization network, we propose a geological-physical-chemical model with some constraints originated from the comprehensive analysis. We then use this model to simulate the coupled processes of the structural deformation, thermal transport, fluid flow and the chemical reaction. The obtained results indicate that the model is efficient in further analyzing the temporal-spatial evolutional trail of the tectonic regime in Jiaodong ore cluster area and in further understanding the nature of the mass metallogensis.
机译:本文根据胶东矿区的构造机制研究进展以及华北东部中生代的相关构造机制转变,首先总结了一些需要进一步研究的关键问题。然后,我们提出一种解决这些问题的方法。众所周知,胶东矿区的金矿具有不同的矿化方式,空间分布和地质环境,可能是中生代一次或多次地质事件的结果。到目前为止,这种对时间演化和空间迁移序列的研究,特别是对上述事件的地球动力学机制的研究还远远不够。此外,定量描述构造动力机制的作用方式和时空框架,以及制定每种构造动力机制对成矿作用的相对贡献,仍然是地质学家研究胶东矿团簇区形成的挑战。根据对区域构造分析的解释,构造动力学,成矿网络的观察和勘探,提出了综合分析引起的一些约束的地质-物理-化学模型。然后,我们使用该模型来模拟结构变形,热传递,流体流动和化学反应的耦合过程。所得结果表明,该模型在进一步分析胶东矿区构造构造的时空演化轨迹以及进一步了解成矿物质的性质方面是有效的。

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